地震地质 ›› 2003, Vol. 25 ›› Issue (4): 647-654.

• 研究论文 • 上一篇    下一篇

西部地区特大地震活动特征及其对大华北地震趋势的影响

陈宇卫, 张军, 闫素萍, 庆梅   

  1. 安徽省地震局, 合肥, 230031
  • 收稿日期:2002-10-02 修回日期:2003-06-29 出版日期:2003-12-03 发布日期:2009-10-26
  • 作者简介:陈宇卫,女,1954年出生,1980年毕业于中国科学技术大学地球物理系,研究员,主要从事地震预报和地震活动性研究,电话:0551-5561093.
  • 基金资助:
    安徽省地震科研基金重点项目(G351007)资助.

CHARACTERISTICS OF GREAT EARTHQUAKE ACTIVITY IN WEST CHINA AND ITS INFLUENCE ON SEISMIC TENDENCY IN NORTH CHINA

CHEN Yu-wei, ZHANG Jun, YAN Su-ping, QING Mei   

  1. Seismological Bureau of Anhui Province, Hefei 230031, China
  • Received:2002-10-02 Revised:2003-06-29 Online:2003-12-03 Published:2009-10-26

摘要: 在分析1900年以来中国大陆西部特大地震(MS≥7.5)的时空分布特征的基础上,进一步研究了大陆西部特大地震与大华北地区强震(MS≥6.0)活动的相关特征,结果表明:地震构造对西部的强震活动显示出很强的控制力;大华北强震与西部特大地震具有同步活动特点,但滞后于西部的地震活动;西部特大地震第3活跃时段已经开始,但大华北地区出现6级以上地震的连发还为时尚早。

关键词: 地震相关活动, 地震趋势, 中国西部, 大华北

Abstract: Based on the analysis of temporal and spatial distribution of great earthquakes (MS≥7.5) in West China since 1900, the correlation between great earthquake activity in West China and strong earthquake (MS≥6.0) activity in North China is studied. The result shows that the activity of great earthquakes in West China is controlled by the seismotectonics of the region. Seismic activities in each active period of great earthquake in West China almost occur successively or in cluster within the same sub plate, but other tectonic units in surrounding areas still keep relatively quiet. This may indicate that a seismically active block is an active tectonic unit confined by boundary faults of various strikes. The activation of strong earthquake on a boundary fault will affect the stability of the other boundary faults within the same tectonic unit, and it may trigger strong earthquake activities on those boundary faults. Seismic activities in China have the characteristics of oriented migration. In the first active period, strong earthquakes concentrated mostly in Xingjiang sub-plate, northwest China. In the early stage of the second active period, the earthquake site migrated to the southwest of Qinghai-Tibet sub-plate, while in the later stage it migrated to the southern part of the South-north seismic belt. In the third active period, the earthquake site migrated to the northwest of Qinghai Tibet sub plate. The earthquakes have no repeatability in spatial distributions. When a series of earthquakes occur in a tectonic block, the last earthquake always migrates from the block and occurs in another relatively stable block, and hence is useful for determining the occurrence site of the next series of earthquakes. The activity of strong earthquakes in North China is basically synchronous with the activity of great earthquakes in West China, but the beginning time of strong earthquake activity in North China is later than that in West China. Therefore, though the third active period of great earthquakes in West China has begun now, the probability of the successive occurrences of strong earthquakes (MS≥6.0) in North China in the near future is very low.

Key words: correlation of seismicity, seismic tendency, West China, North China

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